Isostatic Uplift
Isostatic Uplift is a geophysical process of crustal elevation resulting from the upward adjustment of the lithosphere in response to the removal of surface loads, such as ice or sediment, driven by gravitational equilibrium between the crust and the underlying mantle.
174
Publications
8.7K
Citations
458
Authors
225
Institutions
Publications per year
2017–2026
15
Variants
Isostatic Rebound
174
Recent Ice-Sheet Growth in the Interior of Greenland
Ola M. Johannessen, K. Khvorostovsky, Martin W. Miles et al. · Science · 2005 · 176 citations
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458
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225
United States Geological Survey
Reston, United States
10 h-index
15 publications
1K citations

Stockholm University
Stockholm, Sweden
7 h-index
9 publications
407 citations
UiT The Arctic University of Norway
Tromsø, Norway
5 h-index
11 publications
632 citations

British Antarctic Survey
Cambridge, United Kingdom
5 h-index
12 publications
629 citations

University of Helsinki
Helsinki, Finland
5 h-index
13 publications
414 citations

Centre National de la Recherche Scientifique
Paris, France
5 h-index
12 publications
543 citations

Université Laval
Québec, Canada
5 h-index
14 publications
1.1K citations
Center for Northern Studies
Québec, Canada
4 h-index
14 publications
1.3K citations
1–8 of 225
JGR · 12 publications · 758 citations
12
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10 publications · 481 citations
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7 publications · 282 citations
7
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7 publications · 451 citations
7
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6 publications · 163 citations
6
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1–5